FREE BOOKS

Author's List




PREV.   NEXT  
|<   33   34   35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57  
58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   >>   >|  
f the plateau. The rivers have deep valleys with steep sides and do not furnish arable valley floors; most of the grazing and farming are done on the flatter mountaintops. The rivers provide little access into the area and are barriers to communication within it. Roads are few and poor. Lacking internal communications and external contacts, a tribal society flourished within this Alpine region for centuries. Only after World War II were serious efforts made to incorporate the people of the region into the remainder of the country. Southern Mountains The extent of the region occupied by the southern mountains is not settled to the satisfaction of all authorities. Some include all of the area in a large diamond shape roughly encompassing all the uplands of southern Albania beneath lines connecting Vlore, Elbasan, and Korce. Although this area has trend lines of the same type and orientation, it includes mountains that are associated more closely with the systems in the central part of the country. Other authorities confine the area to the mountains that are east of Vlore and south of the Vijose River. These have features generally common to southern Albania and the adjacent Greek Epirus. This demarcation is considered preferable because it more nearly defined a traditional area that tends to lose some of the more purely national character of the lands north of it. The southern ranges revert again to the northwest to southeast trend lines characteristic of the Dinaric Alps. They are, however, more gentle and accessible than the serpentine zone, the eastern highlands, or the North Albanian Alps. Transition to the lowlands is less abrupt, and arable valley floors are wider. Limestone is predominant, contributing to the cliffs and clear water along the Albanian Riviera. An intermixture of softer rocks has eroded and become the basis for the sedimentation that has resulted in wider valleys between the ridges than are common in the remainder of the country. This terrain encouraged the development of larger landholdings, thus influencing the social structure of the area (see ch. 5, Social System). [Illustration: Source: Adapted from Norman J. G. Pounds, _Eastern Europe_, Chicago, 1969, p. 824. _Figure 2. Landform Regions in Albania_] Lowlands A low coastal belt extends from the northern boundary southward to about Vlore. It averages less than ten miles deep but widens to about thirty miles in the Elbasan area.
PREV.   NEXT  
|<   33   34   35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57  
58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   >>   >|  



Top keywords:
southern
 

region

 

mountains

 

Albania

 

country

 

valleys

 
remainder
 
arable
 
Elbasan
 

Albanian


common

 

rivers

 

valley

 
authorities
 

floors

 

predominant

 

widens

 

contributing

 

Limestone

 

Transition


coastal

 

abrupt

 

lowlands

 

cliffs

 
Lowlands
 

Riviera

 

characteristic

 

Dinaric

 
boundary
 

southeast


northwest

 

ranges

 
revert
 

gentle

 
eastern
 

highlands

 

extends

 

serpentine

 
northern
 

accessible


thirty
 
intermixture
 

softer

 

Social

 

System

 

Illustration

 
Source
 

social

 

structure

 

Adapted